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Elemental composition of air masses under different altitudes in Azores, central north Atlantic

Authors :
Maria do Carmo Duarte Freitas
H.T. Wolterbeek
B. J. Vieira
Source :
Journal of radioanalytical and nuclear chemistry, 291(1)2012
Publication Year :
2011

Abstract

Between 8th July 2002 and 18th June 2004, aerosol samples were collected in Azores. Their inorganic composition was obtained by neutron activation analysis in order to study the differences of aerosols in two atmo- spheric altitudes of the central north Atlantic: (1) PICO- NARE observatory (Lower Free Troposphere-LFT) at Pico mountain summit (38,4708N, 28,4048W, 2,225 m a.s.l.) in Pico Island, Azores, where air masses from the surrounding continents (Africa, Europe, Central and North America) pass through, carrying aerosols with anthropogenic (Sb, Br, Mo, U, Se and Tb) and/or natural emissions (Fe, Co, La, Na, Sm, Cr, Zn, Hf, K and Th); (2) TERCEIRA-NARE station (Marine Boundary Layer) at Serreta (38,698N, 27,368W, 50 m a.s.l.), in Terceira Island, Azores, where natural aerosols (I, Cl, Na, Br and other soil related ele- ments) are predominant. However, a combined interpreta- tion of the data points out to a co-existence of the anthropogenic elements Sb and Mo, eventually with similar origins as the ones passing Pico Mountain summit. Very high concentrations and enrichment factors for Sb, Mo and Br in LFT, higher than the ones found in other areas, confirm atmospheric long-range transport mainly from the west boundary of north Atlantic; this may indicate eventual accumulation and persistence of those elements in the area due to the presence of Azores high pressures or the Hadley cells effect. A significant correlation between Fe and Yb and the enrichment of rare earth elements (La, Sm, Tb and Yb) and Th in LFT aerosols, both reflect a mineral dust intrusions from north Africa (Sahara and Sahel region).

Details

Language :
English
ISSN :
02365731
Database :
OpenAIRE
Journal :
Journal of radioanalytical and nuclear chemistry, 291(1)2012
Accession number :
edsair.doi.dedup.....9fdd9b80b81c70d696b5910ff472fddb